Metal release from manganese nodules in anoxic seawater and implications for deep-sea mining dewatering operations

ACS ES&T Water
By: , and 

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Abstract

The potential mining of deep-sea polymetallic nodules has been gaining increasing attention due to their enrichment in metals essential for a low-carbon future. To date, there have been few scientific studies concerning the geochemical consequences of dewatered mining waste discharge into the pelagic water column, which can inform best practices in future mining operations. Here, we report the results of laboratory incubation experiments that simulate mining discharge into anoxic waters such as those that overlie potential mining sites in the North Pacific Ocean. We find that manganese nodules are reductively dissolved, with an apparent activation energy of 42.8 kJ mol–1, leading to the release of associated metals in the order manganese > nickel > copper > cobalt > cadmium > lead. The composition of trace metals released during the incubation allows us to estimate a likely trace metal budget from the simulated dewatering waste plume. These estimates suggest that released cobalt and copper are the most enriched trace metals within the plume, up to ∼15 times more elevated than the background seawater. High copper concentrations can be toxic to marine organisms. Future work on metal toxicity to mesopelagic communities could help us better understand the ecological effects of these fluxes of trace metals.

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Publication type Article
Publication Subtype Journal Article
Title Metal release from manganese nodules in anoxic seawater and implications for deep-sea mining dewatering operations
Series title ACS ES&T Water
DOI 10.1021/acsestwater.4c00166
Volume 4
Issue 7
Year Published 2024
Language English
Publisher American Chemical Society
Contributing office(s) Pacific Coastal and Marine Science Center
Description 11 p.
First page 2957
Last page 2967
Other Geospatial Clarion-Clipperton Zone, Pacific Ocean
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